Google

soft 'animals', like clams and such

Generalists eat whatever comes along, while specialists are adapted to one or only a few different foods.

there are 56 miles in googolplex.

no cos no1 knowz evrythink

Well for school or projects I recommend the following:

glogster

symbaloo

voki

and for games (learning games) I recommend:

Coolmath4kids

http://trololololololololololo.com/

Puzzlepirates is an online MMO where you have to do different puzzles to get new ships and things.

Well, first, I'm assuming that you are referring to "googolplex" and not "googleplex" as per your title (which actually refers the the Internet Search Giant Google's Headquarters)

And to find out what a googolplex is, we first define a googol:

1 googol = 1 with 100 zeroes after it = 10 ^ 100

The history behind the naming of the googol came in 1938 when Edward Kasner wrote this number and showed it to his nine year old nephew Milton Sirotta, her response was, as the legend goes, "googol!", and thus the googol came into existence.

Now, what is a googolplex?

Well, 1 googolplex = 1 with a googol zeroes after it = 10 ^ (10 ^ 100)

That's a lot of zeroes!

Google searches for items that are stored on the internet and like any other search engine will display it if it fits the criterion of its search. The trick is to make it come up on or close to the front page using Key words, Phrases,descriptions, links to like sites .e.c.t.

P-waves are type of elastic wave, also called seismic waves, that can travel through gasses (such as sounds), elastic solids and liquids, including the Earth. P-waves can be produced by earthquakes and recorded by seismometers. The name P-wave stands for primary wave, as the P-wave is the fastest among the elastic waves, compared to the S-waves. In isotropic and homogeneous solids, the polarization of a P-wave is always longitudinal; thus, the particles in the solid have vibrations along or parallel to the travel direction of the wave energy. In isotropic and homogeneous solids, the polarization of P-waves is always longitudinal. This means that the particles in the body have vibrations along or parallel to the direction of travel of the wave energy. Earthquake advance warning is possible by detecting the non-destructive primary waves that travel more quickly through the earth's crust than do the destructive secondary and Rayleigh waves. The amount of advance warning depends on the delay between the arrival of the P-wave and other destructive waves, generally on the order of seconds up to about a minute maximum for deep, distant, large quakes. The effectiveness of advance warning depends on accurate detection of the P-waves and compensation for ground vibrations caused by local activity (such as trucks or construction work). Almost all the information available on the structure of the Earth's deep interior is derived from observations of the travel times, reflections, refractions and phase transitions of seismic body waves, or normal modes. Body waves travel through the fluid layers of the Earth's interior, but P-waves are refracted slightly when they pass through the transition between the semisolid mantle and the liquid outer core. As a result, there is a P-wave "shadow zone" between 104° and 140°, where the initial P-waves are not registered on seismometers. In contrast, S-waves do not travel through liquids, rather, they are attenuated.A type of seismic wave, the S-wave, secondary wave, or shear wave (sometimes called an elastic S-wave) is one of the two main types of elastic body waves, so named because they move through the body of an object, unlike surface waves. The S-wave move as a shear or transverse wave, so motion is perpendicular to the direction of wave propagation: S-waves, like waves in a rope, as opposed to waves moving through a slinky, the P-wave. The wave moves through elastic media, and the main restoring force comes from shear effects. These waves are divergenceless and obey the continuity equation for incompressible media: Its name, S for secondary, comes from the fact that it is the second direct arrival on an earthquake seismogram, after the compressional primary wave, or P-wave. Unlike the P-wave, the S-wave cannot travel through the molten outer core of the Earth, and this causes a shadow zone for S-waves opposite to where they originate. They can still appear in the solid inner core: when a P-wave strikes the boundary of molten and solid cores, called the Lehmann discontinuity, S-waves will then propagate in the solid medium. And when the S-waves hit the boundary again they will in turn create P-waves. In fact, this property allows seismologists to determine the nature of the inner core. The velocity of an S-wave in an isotropic medium can be described by the shear modulus μ and density ρ. As transverse waves, S-waves exhibit properties, such as polarization and birefringence, much like other transverse waves. S-waves polarized in the horizontal plane are classified as SH-waves. If polarized in the vertical plane, they are classified as SV-waves. When an S- or P-wave strikes an interface at an angle other than 90 degrees, a phenomenon known as mode conversion occurs. As described above, if the interface is between a solid and liquid, S becomes P or vice versa. However, even if the interface is between two solid media, mode conversion results. If a P-wave strikes an interface, four propagation modes may result: reflected and transmitted P and reflected and transmitted SV. Similarly, if an SV-wave strikes an interface, the same four modes occur in different proportions. The exact amplitudes of all these waves are described by the Zoeppritz equations, which in turn are solutions to the wave equation. In elastodynamics, Love waves are essentially horizontally polarized shear waves (SH waves) guided by an elastic layer, which is "welded" to an elastic half space on one side while bordering a vacuum on the other side. In seismology, Love waves (also named Q waves (Quer: German for lateral)) are surface seismic waves that cause horizontal shifting of the earth during an earthquake. A.E.H. Love predicted the existence of Love waves mathematically in 1911; the name comes from him (Chapter 11 from Love's book "Some problems of geodynamics", first published in 1911). They form a distinct class, different from other types of seismic waves, such as P-waves and S-waves (both body waves), or Rayleigh waves (another type of surface wave). Love waves travel with a slower velocity than P- or S- waves, but faster than Rayleigh waves. The particle motion of a Love wave forms a horizontal circle or ellipse moving in the direction of propagation. Moving deeper into the material, motion decreases to a "node" and then alternately increases and decreases as one examines deeper layers of particles. The amplitude, or maximum particle motion, decreases rapidly as one examines deeper layers of particles. Since Love waves travel on the Earth's surface, the strength (or amplitude) of the waves decrease exponentially with the depth of an earthquake. However, given their confinement to the surface, their amplitude decays only as, where r represents the distance the wave has traveled from the earthquake. Surface waves therefore decay more slowly with distance than do body waves, which travel in three dimensions. Large earthquakes may generate Love waves that travel around the Earth several times before dissipating. Love waves take a long time to dissipate due to the huge amount of energy that they contain. For this reason, they are most destructive within the immediate area of the focus or epicentre of an earthquake. They are what most people feel directly during an earthquake. In the past, it was often thought that animals like cats and dogs could predict an earthquake before it happened. However, they are simply more sensitive to ground vibrations than humans and able to detect the subtler waves that precede Love waves, like the P-waves and the S-waves.

853 passengers and 20 crew

Nobody's perfect.

Animators compile models in key poses for the Riggers to bind together and fill the in between frames within the animation sequence.

The models and/or ideas will come from the artists/ clients. Good communication and regular meetings and feedback will increase the quality of the output.

November 2006

US $ 1,65 billion

HPQ on the NYSE

Go to "My Documents", click "My Google Gadgets", and locate the name of the gadget. Open it and it will automatically come back into the sidebar.

Google Sketch-Up is a Google program that is basically Microsoft Paint in a more complicated way. I would definitely not recommend it.

Google Ltd is infact a limited company and therfore not a PLC or party legitimate center

Google is investing in a company that plans to launch 16 satellites whose purpose will be to bring high-speed Internet access to parts of the world that have none. The group, O3b, hopes to launch its service by the end of 2010.

Yes! there are pictures of the tabon men. We have lots of them if you want to see the pictures just click Tabon Men pictures below "Is one of these your question?". "JUST GO TO WWW.WIKIANSWERS.COM AND TYPE ARE THERE ANY PICTURES OF TABON MEN?"

You just have to search it

code of ethics for information technology

No. Affiliate programs will give you a share of the revenue when a user that you direct to their site makes a purchase, or pay you a set amount when a user registers for their service. Earning money from Google AdSense does not require that your users take an action such as purchasing or registering. You simply get paid per click for every user that clicks on the ad; what they do once they arrive at the site does not matter.

If you want to advertise your gambling site you can do it through television and internet both.

But if you are advertising for your site on TV in US you can only advertise .Net version of the site only then it will be allowed, .Com version can't be advertised on television.

It's not as easy as you think. But, I would suggest signing up for Google Adwords, they should supply you with a free search engine for your site. Or, you could always create your own HTML Code that will search your site, but this is extremely difficult so I wouldn't recommend it. Hope this helps! -jjshammas

Google Lively is an online virtual community provided by Google, where you can create your own avatar, virtual space, as well as chat in virtual chat rooms.

Gmail can hold the largest files.